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Carbon and nitrogen budget evaluation of natural and managed ecosystems.

机译:天然和管理生态系统的碳和氮预算评估。

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Components of the annual carbon and nitrogen budgets were evaluated for a natural restored tallgrass prairie and fertilized and unfertilized, no-tillage and chisel plow corn agroecosystems for a four year period. The natural prairie and corn agroecosystems are located near Arlington, Wisconsin and reside on Plano silt loam soil (fine-silty, mixed, mesic Typic Argiudoll). Inorganic nitrogen and dissolved carbon leaching losses were quantified in-situ using equilibrium-tension lysimeters. Inorganic nitrogen leaching was a negligible component of the nitrogen balance for the natural prairie, however nitrogen leaching was a significant component of the nitrogen balance for the fertilized agroecosystems. Dissolved carbon leaching was greatest for the fertilized chisel plow agroecosystem and smallest for the natural prairie. Denitrification was assumed negligible for all ecosystems. However, large net nitrogen mineralization field measurements for the agroecosystems suggested that denitrification may be a significant export of nitrogen from the agroecosystems since leaching losses could not alone reconcile the differences between the inputs and outputs of nitrogen to the fertilized agroecosystems. Soil surface carbon dioxide emissions from the prairie were significantly higher than carbon dioxide emissions from the agroecosystems. High soil respiration fluxes contributed to the nature of the restored prairie being a net carbon source rather than a net carbon sink. Carbon leaching was a minor component of the carbon budgets for both the prairie and agroecosystems. Compared to the prairie, the fertilized agroecosystems were less efficient or leaky in terms of carbon assimilated per unit nitrogen leached. Computer modeling of soil biogeochemical cycling complemented field measurements and provided valuable insight into the mechanisms contributing to and controlling such important processes as nitrate leaching from the rooting zone of fertilized crops.
机译:对四年恢复的天然草木草原,施肥和未施肥,免耕和凿犁玉米农业生态系统的年度碳和氮预算进行了评估。天然草原和玉米农业生态系统位于威斯康星州的阿灵顿附近,居住在普莱诺粉质壤土上(细粉质,混合型,中型Typic Argiudoll)。无机氮和溶解碳的淋失量通过平衡张力溶渗仪就地进行定量。对于自然大草原,无机氮的淋失是氮平衡的可忽略不计的组成部分,但是对于施肥的农业生态系统,氮的淋溶是氮平衡的重要组成部分。受精凿犁农业生态系统中溶解碳的淋溶最大,而天然草原的溶碳淋溶最小。假定反硝化对于所有生态系统都是微不足道的。但是,对农业生态系统进行的大量净氮矿化实地测量表明,反硝化可能是农业生态系统中氮的重要出口,因为浸出损失无法单独调和施肥农业生态系统氮素输入和输出之间的差异。草原的土壤表面二氧化碳排放量明显高于农业生态系统的二氧化碳排放量。较高的土壤呼吸通量有助于恢复草原的性质,即其为净碳源而不是净碳汇。对于草原和农业生态系统而言,碳浸出只是碳预算的一小部分。与大草原相比,施肥的农业生态系统的效率或渗漏率较低(以每单位渗氮吸收的碳计)。土壤生物地球化学循环的计算机建模补充了田间测量,并为有助于和控制重要过程(例如从受精作物生根区浸出硝酸盐)的机制提供了宝贵的见识。

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